Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6934
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dc.contributor.authorallLorito, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallRomano, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallAtzori, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallTong, X.; Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093-0225, USAen
dc.contributor.authorallAvallone, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallMcCloskey, J.; Environmental Sciences Research Institute, School of Environmental Sciences, University of Ulster, Coleraine BT52 1SA, Northern Irelanden
dc.contributor.authorallCocco, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallBoschi, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italiaen
dc.contributor.authorallPiatanesi, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2011-02-08T08:23:16Zen
dc.date.available2011-02-08T08:23:16Zen
dc.date.issued2011-01en
dc.identifier.urihttp://hdl.handle.net/2122/6934en
dc.description.abstractThe MW 8.8 mega-thrust earthquake and tsunami that occurred on February 27, 2010, offshore Maule region, Chile, was not unexpected. A clearly identified seismic gap existed in an area where tectonic loading has been accumulating since the great 1835 earthquake experienced and described by Darwin during the voyage of the Beagle. Here we jointly invert tsunami and geodetic data (InSAR, GPS, land-level changes), to derive a robust model for the co-seismic slip distribution and induced co-seismic stress changes, and compare them to past earthquakes and the pre-seismic locking distribution. We aim to assess if the Maule earthquake has filled the Darwin gap, decreasing the probability of a future shock . We find that the main slip patch is located to the north of the gap, overlapping the rupture zone of the MW 8.0 1928 earthquake, and that a secondary concentration of slip occurred to the south; the Darwin gap was only partially filled and a zone of high pre-seismic locking remains unbroken. This observation is not consistent with the assumption that distributions of seismic rupture might be correlated with pre-seismic locking, potentially allowing the anticipation of slip distributions in seismic gaps. Moreover, increased stress on this unbroken patch might have increased the probability of another major to great earthquake there in the near future.en
dc.language.isoEnglishen
dc.publisher.nameNature Publishing Groupen
dc.relation.ispartofNature Geoscienceen
dc.relation.ispartofseries/4 (2011)en
dc.subjectSource processen
dc.subjectChileen
dc.subjectTsunamien
dc.subjectJoint Inversionen
dc.subjectSeismic Gapen
dc.titleLimited overlap between the seismic gap and coseismic slip of the great 2010 Chile earthquakeen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber173-177en
dc.identifier.URLhttp://www.nature.com/ngeo/journal/vaop/ncurrent/abs/ngeo1073.htmlen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.05. Stressen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.06. Subduction related processesen
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.03. Inverse methodsen
dc.identifier.doi10.1038/ngeo1073en
dc.relation.referencesBarrientos, S. Is the Pichilemu–Talcahuano (Chile) a seismic gap? Seismol. Res. Lett. 61, 43 (1990). Campos, J., & Kausel, E. The large 1939 intraplate earthquake of Southern Chile. Seismol. Res. Lett., 61, 43 (1990). Madariaga, R. La seismicidad de Chile, Fisica de la Tierra, vol. 10. (Ediciones de la Universidad Complutense de Madrid, pp. 221–258, 1998). Beck, S., Barrientos, S., Kausel, E., & Reyes, M. Source characteristics of historic earthquakes along the central Chile subduction zone. J. South Am. Earth Sci. 11, 115–129 (1998). Klotz, J. et al. Earthquake cycle dominates contemporary crustal deformation in Central and Southern Andes. Earth Planet. Sc. Lett., 193, 437-446 (2001). Ruegg, J.C. et al. Interseismic strain accumulation in south central Chile from GPS measurements, 1996–1999. Geophys.Res.Lett., 29, 1517-1520 (2002). Campos, J. et al. A seismological study of the1835 seismic gap in South Central Chile. Phys. Earth Planet. Int. 132, 177–195 (2002). Brooks, B.A. et al. Crustal motion in the Southern Andes (26°–36°S): Do the Andes behave like a microplate? Geochem. Geophys. Geosyst., 4, 1085-1098 (2003). Moreno, M.S., Klotz, J. Melnick, D, Echtler, H. & Bataille, K. Active faulting and heterogeneous deformation across a megathrust segment boundary from GPS data, south central Chile (36–39°S). Geochem. Geophys. Geosyst., 9, Q12024-12037 (2008). Vigny, C. et al. Upper plate deformation measured by GPS in the Coquimbo Gap, Chile. Phys. Earth Planet. In. 175, 86-95 (2009). Ruegg, J.C. et al. Interseismic strain accumulation measured by GPS in the seismic gap between Constitución and Concepción in Chile. Phys. Earth Planet. In. 175, 78–85 (2009). Madariaga, R., Métois, M., Vigny, C., & Campos, J. Central Chile Finally Breaks. Science, 328, 181-182 (2010). Moreno M., Rosenau M., & Oncken O. 2010 Maule earthquake slip correlates with pre-seismic locking of Andean subduction zone. Nature, 467, 198-204 (2010). Darwin, C. Journal of the researches into the natural history and geology of the countries visited during the voyage of the HMS Beagle round the world: London, John Murray, 2ed (1845). Farías M. et al. Land-Level Changes Produced by the Mw 8.8 2010 Chilean Earthquake. Science, 329, 916 (2010). Delouis, B., Nocquet J.-M., & Vallée M. Slip distribution of the February 27, 2010 Mw=8.8 Maule Earthquake, central Chile, from static and high-rate GPS, InSAR, and broadband teleseismic data. Geophys. Res. Lett., 37, L17305 (2010). Lay, T. et al. Teleseismic inversion for rupture process of the 27 February 2010 Chile (Mw 8.8) earthquake. Geophys. Res. Lett., 37, L13301 (2010). Tong, X. et al. The 2010 Maule, Chile earthquake: Downdip rupture limit revealed by space geodesy. Geophys. Res. Lett., in press, 2010. Moreno, M. S., Bolte, J. Klotz, J. & Melnick D. Impact of megathrust geometry on inversion of coseismic slip from geodetic data: Application to the 1960 Chile earthquake. Geophys. Res. Lett., 36, L16310 (2009). Konca, O. et al. Partial rupture of a locked patch of the Sumatra megathrust during the 2007 earthquake sequence. Nature, 456, 631–635 (2008). Bilek, S. L. The role of subduction erosion on seismicity. Geology, 38(5), 479 (2010). Nalbant, S.S., Steacy, S., Sieh, K., Natawidjaja, D. & McCloskey, J. Earthquake risk on the Sunda trench. Nature, 435, 756-757 (2005). Lichten, S. & Borders, J. Strategies for High-Precision Global Positioning System Orbit Determination. J. Geophys. Res., 92, 12751-12762 (1987). D'Agostino, N. et al. Active tectonics of the Adriatic region from GPS and earthquake slip vectors. J. Geophys. Res., 113, B12413 (2008). Altamimi, Z., Collilieux, X., Legrand, J., Garayt, B. & Boucher, C. ITRF2005: A new release of the International Terrestrial Reference Frame based on time series of station positions and Earth Orientation Parameters. J. Geophys. Res., 112, B09401 (2007). Bird, P. An updated digital model of plate boundaries. Geochem. Geophys. Geosyst., 4(3), 1027 (2003). Okada, Y. Surface deformation due to shear and tensile faults in a half-space. Bull. Seismol. Soc. Am., 75, 1135 – 1154, (1985). Lorito, S., Piatanesi, A., Cannelli, V., Romano, F., & Melini, D. Kinematics and source zone properties of the 2004 Sumatra-Andaman earthquake and tsunami: Nonlinear joint inversion of tide gauge, satellite altimetry, and GPS data. J. Geophys. Res., 115, B02304, (2010). Lin, J., & Stein, R.S. Stress triggering in thrust and subduction earthquakes, and stress interaction between the southern San Andreas and nearby thrust and strike-slip faults. J. Geophys. Res., 109, B02303 (2004). Toda, S., Stein, R.S., Richards-Dinger, K. & Bozkurt, S. Forecasting the evolution of seismicity in southern California: Animations built on earthquake stress transfer. J. Geophys. Res., 110, B05S16 (2005).en
dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.obiettivoSpecifico4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.contributor.authorLorito, S.en
dc.contributor.authorRomano, F.en
dc.contributor.authorAtzori, S.en
dc.contributor.authorTong, X.en
dc.contributor.authorAvallone, A.en
dc.contributor.authorMcCloskey, J.en
dc.contributor.authorCocco, M.en
dc.contributor.authorBoschi, E.en
dc.contributor.authorPiatanesi, A.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentInstitute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093-0225, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentEnvironmental Sciences Research Institute, School of Environmental Sciences, University of Ulster, Coleraine BT52 1SA, Northern Irelanden
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptInstitute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093-0225, USA-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptUniversity of Ulster,Coleraine, Northern Ireland-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0002-1458-2131-
crisitem.author.orcid0000-0003-2725-3596-
crisitem.author.orcid0000-0002-5031-9904-
crisitem.author.orcid0000-0002-0264-2897-
crisitem.author.orcid0000-0001-6798-4225-
crisitem.author.orcid0000-0003-2863-3662-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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